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Are there any circumstances in which logging primary wet-eucalypt forest will not add to the global carbon burden?
Citation
Dean, C and Wardell-Johnson, GW and Kirkpatrick, JB, Are there any circumstances in which logging primary wet-eucalypt forest will not add to the global carbon burden?, Agricultural and Forest Meteorology: An International Journal, 161 pp. 156-169. ISSN 0168-1923 (2012) [Refereed Article]
Copyright Statement
Copyright 2012 Elsevier
DOI: doi:10.1016/j.agrformet.2012.03.021
Abstract
Uncertainty associated with past land-use emissions restricts quantification of climate change effects. We
identify the major affects of commercial forestry initiated over recent decades on Tasmanian primaryforest
carbon (C), and search for means to mitigate its ongoing impacts. Spatio-temporal trends were
derived from records of commercial operations combined with biomass data. Over the last two decades,
the majority of forest C destined for short- or long-term emission (LTE, i.e. over several centuries and
multiple harvests) was from clearfelling the higher-biomass wet-eucalypt forests on public land. Carbon
dynamics at the unit-area-level for logging two disparate, wet-eucalypt forests were modelled. Parameters
were varied to determine management options and model sensitivities under conversion by clearfell
and intense burn to either eucalypt plantation or forest regeneration from local eucalypt seed. The first
cycle of conversion of primary-forests contributed 43(±5)% to the LTE, and the LTE constituted
∼50%
of the primary-forest C stock. Whether the first logging of even-aged primary-forests was prior to or
after maturity, the LTEs were equivalent, although short-term emissions (STEs) were ∼2× higher from
old-growth. Minor variations in soil organic carbon efflux during operations significantly altered LTEs.
Conversion of wet-eucalypt by clearfell from 1999 to 2009 incurred an LTE of 2(±1.6) Tg from each year’s
logging. Lengthening the harvesting interval for sown forests from 80 to 200 years reduced LTEs by 42%
and eucalypt wood-products by 26%; but yielded 40(±20) Mg ha−1 of C in rainforest understorey—helping
to sustain mixed-forest ecosystems and their products. Using 200-yr cycles for the wet-eucalypt already
clearfelled could avoid LTEs of
∼15 Tg. Long-term C dynamics under harvest cycles were constrained by
mathematical precepts that facilitate climate change modelling, e.g. the time to reach the harvestingcycle’s
asymptote is correlated to the half-life of the longer-lived C pool. Emissions are not recovered
by sequestration in wood-products unless their half-lives are
∼10×
contemporary values—requiring
200–1000 years for recovery, during which time emissions would augment global climate change. Emissions
can be reduced by product substitution, and by recycling wood-products, in a stable wood market.
Primary-forest is part of a global commons. Comprehensive C accounting cannot occur if logging effects
are omitted.
Item Details
Item Type: | Refereed Article |
---|---|
Keywords: | carbon sequestration, carbon emission, clearfell, old-growth, wood products, climate change positive feedback |
Research Division: | Earth Sciences |
Research Group: | Climate change science |
Research Field: | Climate change processes |
Objective Division: | Environmental Management |
Objective Group: | Fresh, ground and surface water systems and management |
Objective Field: | Assessment and management of freshwater ecosystems |
UTAS Author: | Dean, C (Dr Christopher Dean) |
UTAS Author: | Kirkpatrick, JB (Professor James Kirkpatrick) |
ID Code: | 81090 |
Year Published: | 2012 |
Web of Science® Times Cited: | 17 |
Deposited By: | Geography and Environmental Studies |
Deposited On: | 2012-11-22 |
Last Modified: | 2017-10-30 |
Downloads: | 0 |
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